{"refrec":{"BRefID":209212,"RR":"<b>Moernaut, J.; De Batist, M.; Heirman, K.; Van Daele, M.; Pino, M.; Brümmer, R.; Urrutia, R.</b> (2009). Fluidization of buried mass-wasting deposits in lake sediments and its relevance for paleoseismology: Results from a reflection seismic study of lakes Villarrica and Calafquén (South-Central Chile). <i>Sediment. Geol. 213(3-4)</i>: 121-135. <a href=\"http://dx.doi.org/10.1016/j.sedgeo.2008.12.002\" target=\"_blank\">dx.doi.org/10.1016/j.sedgeo.2008.12.002</a>","BEntID":201198,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Sediment. Geol. 213(3-4)</i>: 121-135. <a href=\"https://dx.doi.org/10.1016/j.sedgeo.2008.12.002\" target=\"_blank\">https://dx.doi.org/10.1016/j.sedgeo.2008.12.002</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Moernaut, J.; De Batist, M.; Heirman, K.; Van Daele, M.; Pino, M.; Brümmer, R.; Urrutia, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Moernaut, J. <i>et al.</i>","Englishabstract":"A dense grid of very-high resolution seismic profiles on Lake Villarrica provides a quasi-3D view on intercalated lenses of low-amplitude reflections, which are connected by acoustic wipe-out patches and fractures to an underlying voluminous mass-wasting deposit. The lenses are interpreted as being created by earthquake-triggered liquefaction in this buried mass-wasting deposit and subsequent sediment fluidization and extrusion at the paleo-lake bottom. These sediment volcanoes are mapped in detail. They have a rather uniform circular geometry and show a linear relationship between apparent width and maximum thickness on a seismic section. The largest sediment volcanoes are up to 80 m wide and 1.9 m thick. Their slope angles designate a syn- to post-depositional sagging of most sediment volcanoes. Sediment volcano detection and mapping from nearby Lake Calafquén further strengthen the revealed geometrical relationships. Locally, some of the sediment/fluid escape structures extend to a higher position in the stratigraphy, which points to a polyphase escape process associated with multiple multi-century spaced strong earthquakes. Thickness and morphology of the source layer seem to exert a dominant control in the production of sediment/fluid extrusions. This study shows that reflection seismic profiling allowed recognizing 4 different seismic events in the studied stratigraphic interval, which are evidenced by mass-wasting deposits and/or fluidization features.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Fluidization of buried mass-wasting deposits in lake sediments and its relevance for paleoseismology: Results from a reflection seismic study of lakes Villarrica and Calafquén (South-Central Chile)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Fluidization structures; Lake sediments; Reflection seismic profiling; South-Central Chile; Paleoseismology","OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2014-10-09","DateCreate":"2011-11-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000264144400005","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.sedgeo.2008.12.002"},"refs":null,"anarec":{"AnaID":209212,"PubliDate":2009,"Pagination":"121-135","XtraPublOfAnaID":null,"ISBN":null,"Volume":"213","Issue":"3-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43811,"SerRR":"Sedimentary Geology. Elsevier: Tokyo; Oxford; New York; London; Amsterdam.  ISSN 0037-0738; e-ISSN 1879-0968","StandardTitleSer":"Sedimentary Geology","ISSN":"0037-0738","AbbrevSer":"Sediment. 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